Deltaic
Progradation During Maximum Marine Transgression, the Heebner Shale Member of the Oread Limestone Formation (Virgilian), Southeast Kansas and Northeast Oklahoma
W. Yang, M. Bruemmer, and M. Turnerwilliams
Department of Geology, Wichita State
University, Wichita, KS ([email protected])
The widespread Heebner Shale of the Pennsylvanian Oread Cyclothem
was deposited on the Kansas shelf and adjacent basins in a
paleoequatorial belt during a maximum marine flooding. It overlies
persistent and thin (~50 cm) transgressive Leavenworth Limestone
and underlies persistent but variably thick (0–8 m) regressive Plattsmouth
Limestone along a 120-km outcrop in southeastern Kansas
and northeast Oklahoma. In the northern and central outcrop belt,
the Heebner is thin (1–3 m) and dominantly black with abundant
phosphatic nodules, representing a condensed section deposited on
an anoxic to dysaerobic starved shelf. In the southern belt, however,
the Heebner thickens to 30 m over a distance of 30 km and consists
of upward-coarsening green-gray plant-rich shale, siltstone, and sandstone,
deposited in prodeltaic to delta-front
environments
. The delta
was sourced by the Ouachita thrustbelts and prograded across the
filled Arkoma Basin during maximum flooding and sea-level highstand.
The sediment yield in the source area was copious because of
efficient weathering due to the humid equatorial climate and the
high topographic relief. Sediment transport was efficient due to the
low wave energy in the inland sea, the large river discharge, and the
steep topographic gradient between the source area and depositional
site. The large river runoff also contributed to shelf anoxia by freshwater
capping dense oceanic water, causing stagnant oceanic circulation.
The findings are not predicted by the depositional sequence
model and signify the interplay of oceanic and climatic processes,
sediment yield and sediment supply, and topography of drainage basins
during sequence formation.
AAPG Search and Discovery Article #90903©2001 AAPG Mid-Continent Meeting, Amarillo, Texas